A cirrostratus cloud is a high, thin, generally uniform stratiform type composed of ice-crystals. It is difficult to detect and is capable of forming halos when the cloud takes the form of thin cirrostratus nebulosus.
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Cirrus clouds are high-altitude clouds that are thin, wispy, and composed of ice crystals. They often form at elevations above 20,000 feet and are commonly seen in fair weather, indicating stable atmospheric conditions. Cirrus clouds can be seen streaking the sky with their delicate, feathery appearance.
Cirrus clouds are very thin and wispy clouds that don't produce rain. It was named after the Latin word for curly hair.
They look like fish scales. They can indicate unsettled weather. Often called a mackerel sky
Cirrus clouds are primarily made out of ice crystals.
No clouds are higher than cirrus clouds. Cirrus clouds are the highest clouds in the atmosphere and are typically found at altitudes above 20,000 feet.
Cirrus clouds are typically higher in the sky than cumulus clouds. Cirrus clouds form at higher altitudes, usually above 20,000 feet, while cumulus clouds form at lower altitudes, typically below 6,500 feet.
An alto cirrus cloud is a type of cloud that forms at high altitudes, typically above 20,000 feet. These clouds are composed of ice crystals and have a wispy appearance. Alto cirrus clouds are often thin and wispy in structure, resembling delicate feathers or streaks in the sky.
The term "alto cirrus" is incorrect because it combines two cloud types, altostratus and cirrus, that have different characteristics and altitudes in the sky. Altostratus clouds are mid-level layered clouds, while cirrus clouds are high-level wispy clouds. It is important to use the correct terminology to accurately describe cloud types.